英语词汇“forearc”的音标、意思、用法及中文翻译-反思网

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The inner trench wall marks the edge of the overriding plate and the outermost forearc.
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Methane is often sequestered in an ice-like form (methane clathrate, also called gas hydrate) in the forearc.
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In early stages of arc-continent collision, there is uplift and erosion of the accretionary prism and forearc basin.
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The erosive properties of these volcanoes are consistent with the metamorphic grades (blueschists) expected for this region in the forearc.
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Note that at this early stage the forearc region is a relatively quiet region from a structural point of view.
A faultcontrolled forearc basin was initiated at the back of the prism.
Ophiolitederived clasts within the inner fan part of the forearc siliciclastic submarine fan suggest the outer arc as an important sediment source.
Tectonic processes have played a major role in sedimentation patterns within the forearc basin.
Uplift of the accretionary complex and its erosion influenced fan development in the adjacent forearc.
Towards the end of forearc deposition the shallowing of the basin favoured carbonate deposition.
Shelved and benched forearc basin morphologies are host to some of the thickest successions of basin strata.
The oblique plate motion was resolved into trench normal subduction and dextral movements, which generated strike-slip faults and developed the forearc basin in this part of the subduction complex.
Palaeocurrent data and facies distributions indicate that the continental deposits formed a fanshaped wedge at least 30 km in diameter in the southern part of the forearc basin.
The created ophiolite becomes the tip of the new subductions forearc and is uplifted (over the accretionary wedge) by detachment and compression.
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Over geological time there is constant recycling of the forearc deposits due to erosion, deformation and sedimentary subduction.
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As such, forearc regions are found at convergent margins, and include any accretionary wedge and forearc basin that may be present.
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词汇	forearc
释义	BETA Examples of forearc forearc isn’t in the Cambridge Dictionary yet. You can help! Sediments accreted to the forearc are another source of fluids. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. The inner trench wall marks the edge of the overriding plate and the outermost forearc. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. Methane is often sequestered in an ice-like form (methane clathrate, also called gas hydrate) in the forearc. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. In early stages of arc-continent collision, there is uplift and erosion of the accretionary prism and forearc basin. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. The erosive properties of these volcanoes are consistent with the metamorphic grades (blueschists) expected for this region in the forearc. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. Note that at this early stage the forearc region is a relatively quiet region from a structural point of view. A faultcontrolled forearc basin was initiated at the back of the prism. Ophiolitederived clasts within the inner fan part of the forearc siliciclastic submarine fan suggest the outer arc as an important sediment source. Tectonic processes have played a major role in sedimentation patterns within the forearc basin. Uplift of the accretionary complex and its erosion influenced fan development in the adjacent forearc. Towards the end of forearc deposition the shallowing of the basin favoured carbonate deposition. Shelved and benched forearc basin morphologies are host to some of the thickest successions of basin strata. The oblique plate motion was resolved into trench normal subduction and dextral movements, which generated strike-slip faults and developed the forearc basin in this part of the subduction complex. Palaeocurrent data and facies distributions indicate that the continental deposits formed a fanshaped wedge at least 30 km in diameter in the southern part of the forearc basin. The created ophiolite becomes the tip of the new subductions forearc and is uplifted (over the accretionary wedge) by detachment and compression. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. Over geological time there is constant recycling of the forearc deposits due to erosion, deformation and sedimentary subduction. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license. As such, forearc regions are found at convergent margins, and include any accretionary wedge and forearc basin that may be present. From Wikipedia This example is from Wikipedia and may be reused under a CC BY-SA license.
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Examples of forearc